穿越古冲沟多种地层的隧道初期支护内力及变形规律初探

Preliminary Study on Internal Forces and Deformation Laws of the Initial Support of Railway Tunnels Passing through Various Strata in the Paleogully

  • 摘要: 阳城隧道穿越古冲沟,经历黄土地层、土砂分界地层、全风化红砂岩地层等,施工过程中出现初期支护大变形、开裂等病害。文章基于室内基本力学试验,以现场监控量测为主,辅以数值试验对穿越古冲沟多种地层的隧道支护结构变形及受力特性进行初步探究。研究结果表明:虽然砂质黄土粘聚力更大,但全风化红砂岩的压缩模量和内摩擦角却更大;土砂分界地层的洞周位移值复杂多变,介于砂质黄土地层和全风化红砂岩地层位移值之间。全风化红砂岩地层拱脚处以及土砂分界地层分界面位置处初期支护会出现拉应力,施工时需要加以注意;数值试验变形规律与现场实测结果相同,与黄土地层和红砂岩地层不同,在土砂分界地层中分界面上部初期支护最小主应力要大于其它位置,而分界面处的最大主应力略大于拱脚处。

     

    Abstract: The Yangcheng tunnel mainly passes through the loess stratum, soil-sand interface strata, completely weathered red sandstone stratum, etc. in the paleogully. During the construction, large deformation and cracking of the initial support were encountered. Based on the physical and mechanical tests, field monitoring and measuring as well as the numerical simulation, it studies the deformation and stress behaviors of the initial support structure of the tunnel crossing various strata in the paleogully. The study conclusions are as follows: 1) although the cohesion of sandy loess is larger, the compressive modulus and internal friction angle of the completely weathered red sandstone are larger; 2) the tunnel displacements in the soil-sand interface strata are complex and variable, with the values being still between the displacements in the loess stratum and the completely weathered red sandstone stratum. The tensile stresses would appear at the arch foot in the completely weathered red sandstone stratum and at the interface of the soil-sand strata, which should be paid attention to during construction; 3) the deformation law in the numerical simulation is the same as that in the field test. Unlike conditions in the loess and red sandstone strata, as for the soilsand interface strata, the minimum principal stress at the upper part of the interface is larger than that at other locations, and the maximum principal stress at the interface is slightly larger than that at the arch foot.

     

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